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Karisimbi

Stratovulcano · DR Congo-Rwanda · 4490 m

The Karisimbi volcanic complex (center) includes a symmetrical, peaked summit flanked to the SE by the 2-km-wide Branca caldera, which is filled by viscous lava flows and two craters. The smaller Muntango crater is located S of the summit. A broad lava plain composed of flows erupted within the caldera and along a chain of parasitic cones, extends SW. Eroded Mikeno volcano is at the upper left and Visoke volcano at the upper right of this Landsat image.
The Karisimbi volcanic complex (center) includes a symmetrical, peaked summit flanked to the SE by the 2-km-wide Branca caldera, which is filled by viscous lava flows and two craters. The smaller Muntango crater is located S of the summit. A broad lava plain composed of flows erupted within the caldera and along a chain of parasitic cones, extends SW. Eroded Mikeno volcano is at the upper left and Visoke volcano at the upper right of this Landsat image. · Foto: NASA Landsat image, 1999 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology). · Wikimedia Commons
Tipo
Stratovulcano
Paese
DR Congo-Rwanda
Regione
Eastern Africa Volcanic Regions / Albertine Rift Volcanic Province
Altitudine
4490 m
Coordinate
-1.506, 29.450
Ultima eruzione
-8050
Contesto tettonico
Rift zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Trachybasalt / Tephrite Basanite
Sintesi geologica

Karisimbi is a complex basanitic-to-trachytic volcano with a symmetrical sharp-peaked summit. The 2-km-wide Branca caldera, located SE of the summit, is filled by viscous lava flows and two explosion craters. The large 1.2-km-wide Muntango pit crater is located south of the summit. A broad lava plain, formed from lava flows erupted within the caldera and along a chain of cones, extends SW. More than 100 cones erupted along a NNE-SSW zone that extends to the shores of Lake Kivu. The youngest Potassium-Argon date obtained is about 10,000 years before present (de Mulder, 1985). The youngest eruptions produced a group of dome-shaped vents east of the caldera, which fed viscous lava flows that traveled as far as 12 km E, and lava flows from the SW-flank lava vents.

Sintesi da Wikipedia

Il monte Karisimbi è un vulcano in fase di quiescenza nella catena dei Monti Virunga al confine tra Ruanda e Repubblica Democratica del Congo.

Wikipedia · CC BY-SA · Leggi l'articolo completo

Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
8050 BCE~8050 BCE · 1 eruzioni · VEI max. ?8050 BCE8050 BCE8049 BCE8049 BCE8049 BCE

Cronologia dettagliata

  1. 8050 a.C.VEI ?Stima geologica
    BCE 8050 – In corso

Link esterni

⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.